The last 34 Myr documents the evolution from a unipolar to bipolar world
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Carbonate deposition is an important part of the carbon cycle
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Carbonate deposition in the Atlantic Ocean was poorly understood
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X-Ray Fluorescence Core Scanning unlocks the sediments chemical composition
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We XRF core scanned the entirety of Site 1264 between 2011 and 2018
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The XRF data could help ensure stratigraphic continuity
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CODD: generate composite core photos...
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CODD: ... and composite splice core photos
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We used different tuning approaches from 8-0 Ma because eccentricity was weaker
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The orbital imprint on Caco, deposition shows three distinct phases
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Eccentricity-paced cyclicity (dissolution?) dominates during Miocene warmth
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The MCO may have been preconditioned by early Miocene warmth
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Precession-driven deposition prevails after the mid Miocene climate transition
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High-latitude biomes drove this
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The stronger high-latitude processes coincide with the -8 Ma onset of the LMBB
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The LMBB is globally recognised, but the origins are not yet understood
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The LMBB onset seems synchronous between the Atlantic and the Pacific
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Increased nutrients may come from...
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The global nutrient distribution may reflect regional differences in...
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New insights into the LMBB indicate...
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CODD: Code for Ocean Drilling Data
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Current version CODD 2.1 for IGOR Pro 7 & 8
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A 30 million year CaCO, view of climate, cry and carbon cycle interactions
Description:
Explore a comprehensive 56-minute lecture on the evolution of carbonate deposition patterns in the Southeast Atlantic over the past 30 million years. Delve into XRF core scanning techniques used to approximate carbonate content at Wallis Ridge, and uncover insights into climate, cryosphere, and carbon cycle interactions since the early Oligocene. Examine the transition from a unipolar to bipolar world, the importance of carbonate deposition in the carbon cycle, and the previously understudied Atlantic Ocean carbonate deposition. Learn about the XRF core scanning process conducted at Site 1264 between 2011 and 2018, and how this data ensures stratigraphic continuity. Discover the three distinct phases of orbital imprint on CaCO3 deposition, including eccentricity-paced cyclicity during Miocene warmth and precession-driven deposition after the mid-Miocene climate transition. Investigate the onset of the Late Miocene Biogenic Bloom (LMBB), its global recognition, and potential origins. Gain new perspectives on nutrient distribution and its regional differences. Conclude with an overview of the CODD (Code for Ocean Drilling Data) tool and its application in analyzing 30 million years of CaCO3 data to understand climate, cryosphere, and carbon cycle interactions.
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Disentangling the Controls and Orbital Pacing of SE Atlantic Carbonate Deposition Since the Oligocene